Astrobiology Research Priorities for Primitive Asteroids


Effects of asteroid interactions with the biosphere



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Effects of asteroid interactions with the biosphere

Asteroids and the Late Heavy Bombardment


The flux of small bodies at Earth during the Hadean eon (4.5-3.8 Gy) is of particular interest because Earth’s differentiation had been completed and its surface cooled. The end of this eon is closely linked to the earliest evidence for habitable conditions on our planet (e.g., Mojzsisi et al., 1996). The epoch around 3.9 Gy ago is particularly crucial because of the growing evidence for a large spike in the bombardment rate, the so-called Late Heavy Bombardment (LHB), of the terrestrial planets (Tera et al. 1974, Cohen et al., 2000, Strom et al. 2005). It is likely that the LHB projectiles were asteroids ejected from the main asteroid belt by means of a large scale dynamical instability. It is thought that this instability was related to the orbital migration of the giant planets (Gomes et al. 2005, Strom et al 2005, Levison et al. 2007). Calculations by Minton & Malhotra (2008) have demonstrated that the migration of Jupiter and Saturn would have caused orbital resonances to “sweep” through the asteroid belt, dynamically launching asteroids into the inner Solar System and greatly depleting the asteroid reservoir, possibly by more than 90%. The orbital migration of the giant planets was fueled by about 30 Earth-masses of outer solar system planetesimals (Hahn & Malhotra 1999, Tsiganis et al. 2005), only ~0.1 Earth-masses of which survive in the present-day Kuiper belt. Thus, the LHB was likely a large spike in the flux of both asteroidal and cometary impactors throughout the Solar system. Outstanding questions about this event include:

  • What was the duration of the Late Heavy Bombardment?

  • What was the timescale of the giant planet migration?

  • Was the trigger an orbital instability associated with giant planet orbital resonances or possibly the late formation of Neptune and Uranus?

  • What is the time evolution of the impact flux of asteroids and Kuiper belt objects on the terrestrial planets and outer planet satellites?

  • What were the impact velocities and relative fluxes of asteroids/comets/dust on various Solar System bodies during the Late Heavy Bombardment?

The Impact Hazard


Asteroid impacts have been responsible for mass extinctions in geologic history and remain today the most potentially destructive natural disaster facing humanity. For this reason, it is important to understand the near-Earth asteroid population. Near-Earth asteroids pose a serious and credible threat to humankind. Several such near-Earth objects have only been discovered within days of the objects' closest approach to Earth and recent discoveries of such large objects indicate that many large near-Earth asteroids remain undiscovered. Asteroid collisions rank as one of the most costly natural disasters that can occur. Basic information is needed for technical and policy decision making for the United States to create a comprehensive program in order to be ready to eliminate and mitigate the threats posed by potentially hazardous near-Earth asteroids.

The physical processes that determine the transport of asteroids across the Solar System are dominated by the gravitational dynamics of the major planets, particularly the orbital resonances and dynamical chaos that arise from the long term and long range combined effects of several planets. However, non-gravitational forces, such as due to solar radiation, become increasingly important for smaller size sources. The absorption and reemission of sunlight by small asteroids produces a thermal force, known as the Yarkovsky effect that results in a non-gravitational acceleration and produces a slow but steady drift in the semi-major axis of a NEO’s orbit (Chesley et al. 2003; Bottke et al. 2006). Photon emission thus produces a Sun-powered thrust that can move small asteroids by several AU over their history, pushing them into gravitational resonances or into collisions with planets. The Yarkovsky effect must be fully understood before we can predict the long-term dynamics of potentially hazardous objects with a high degree of fidelity. These concerns are addressed by several key questions:



  • What is the current distribution of near-Earth asteroids?

  • What are the physical characteristics (size, density, internal structure) of the most potentially hazardous asteroids?

  • What is the uncertainty in asteroid positions resulting from insufficient characterization of the Yarkovsky effect?

  • What is the most effective way to mitigate an impact hazard?


Space Missions for the Exploration of Asteroids

Asteroid Sample Return


Spacecraft studies of asteroids have greatly improved our knowledge of these bodies. The most important of these is the complete analyses of the data on 433 Eros returned from the Near Earth Asteroid Rendezvous (NEAR) mission and the successful encounter of the Japanese Hayabusa spacecraft with asteroid Itokawa. These encounters demonstrated the diversity of asteroids and their complexity both internally and on the surface.

An asteroid sample return mission will provide an enormous scientific payoff. Sample return missions have consistently led to paradigm changing results. The Apollo samples revealed the magma-ocean stage of lunar history and the Giant-Impact Hypothesis for the origin of the Earth and Moon. The Genesis mission measured the chemical and isotopic composition of the Sun. The Stardust mission redefined our understanding of early Solar System dynamics. Asteroid sample return is the logical next step in asteroid science.

The highest value sample is pristine carbonaceous material from the early Solar System. In particular such a mission should strive to return material not known to be on Earth. In particular, friable, volatile-rich, and organic-rich material is unlikely to survive passage through the atmosphere and residence on the surface of the Earth. Contamination control and documentation is essential to achieving this objective. Asteroidal samples offer a unique record of the complex chemical evolution that occurred in the early solar nebula. Despite having abundant samples in the form of meteorites, these samples lack geologic context. An asteroid sample return mission would acquire samples with known geologic context

As recommended in the NRC report New Opportunities in Solar System Exploration, such a mission should have the following science objectives:



  • Map the surface texture, spectral properties (e.g., color, albedo) and geochemistry of the surface of an asteroid at sufficient spatial resolution to resolve geological features (e.g., craters, fractures, lithologic units) necessary to decipher the geologic history of the asteroid and provide context for returned samples.

  • Document the regolith at the sampling site in situ with emphasis on, e.g., lateral and vertical textural, mineralogical and geochemical heterogeneity at scales down to the sub-millimeter.

  • Return a sample to Earth in amount sufficient for molecular (or organic) and mineralogical analyses, including documentation of possible sources of contamination throughout the collection, return and curation phases of the mission.



Main-belt Comet Explorer


Comets have been discovered in the asteroid belt. Several members of the Themis asteroid family have been observed to display temporary comet-like activity (Hsieh and Jewitt 2006). Seasonal heating effects in are only sufficient to drive sublimation on these bodies for a portion of their orbits, from the time of perihelion to halfway to aphelion (Hsieh 2007). The recurrent activity of these asteroid-comet transition objects is thought to result from seasonal variations that periodically illuminate ice-rich surfaces. Unlike other known comets, these main belt comets appear to have formed in the much warmer inner Solar System, where they are found today. Orbiting completely within the main asteroid belt, the main belt comets present a distinct contrast with other periodic comets, the Jupiter-family and Halley-family comets, which originate in the cold outer solar system in the Kuiper Belt or Oort Cloud. Main belt comets are more accessible than all other comets, making them excellent targets for a spacecraft investigation. A rendezvous mission to a Main Belt comet would provide monitoring of changes in activity.

Such a mission should have the following science objectives:



  • Rendezvous with the target prior to perihelion and the beginning of cometary activity.

  • Perform thorough global characterization of the texture, spectral properties, mineralogy, and geochemistry of the target during its quiescent period.

  • Measure the shape, mass, and rotation state of the target

  • Measure the internal structure of the target

  • Observe the target through perihelion to document the onset of cometary activity

  • Determine the mechanism for current cometary activity, whether due to recent impacts or fragmentation due to rapid rotation

  • Directly measure the composition of gas and dust liberated from the comet nucleus

  • Analyze the isotropic composition of Main Belt cometary water, and test whether outer Main Belt objects were a major contributor to terrestrial water

  • Observe the target past perihelion to document the cessation of cometary activity


Trojan Reconnaissance


The Trojans, now known to number well over a thousand, are aggregated about the L4 and L5 equilibrium points along Jupiter’s orbit. These objects are asteroids with a low albedo and a featureless, reddish spectrum. They may have been captured in the present orbits during giant planet formation and migration. Trojan asteroids could prove rich in organics, perhaps sampling regions of the nebula and types of organics not sampled on Earth or by previous missions. Detailed study of these objects should greatly expand our understanding of the history of volatiles and organic molecules in the early Solar System.

As recommended in the NRC report New Opportunities in Solar System Exploration, such a mission should have the following science objectives:



  • Determine the physical properties (e.g., mass, size, density) of a Trojan

  • Map the color, albedo, and surface geology of a Trojan at a resolution sufficient to distinguish important features for deciphering the history of the object (e.g., craters, fractures, lithologic units).


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